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- W2901636194 abstract "During the Messinian Salinity Crisis (MSC), between 5.97 and 5.33 Ma, the marine connections between the Atlantic Ocean and the Mediterranean Sea were temporarily restricted. The post-MSC reflooding of the Mediterranean Sea by the Atlantic waters and its sedimentary record are debated. The Boudinar basin (North-Morocco) provides an exceptional record of this period between ca 5.32–5.27 and 4.37 Ma at youngest (Zanclean - Zone PL1). The sedimentary succession of this basin comprises seven facies associations corresponding to depositional settings ranging from continental to open marine environments. We provide a new sequence stratigraphic framework, based on twelve stratigraphic sections. Two orders of depositional sequences (4th, 3rd order), related to base-level changes during the Late-Messinian Early-Pliocene time interval, are correlated at the basin scale. According to our reconstruction, the post-MSC base level rise and the Zanclean reflooding lasted from a minimum of several tens up to hundreds thousands years, suggesting a gradual, not catastrophic event indicative of a progressive transgression." @default.
- W2901636194 created "2018-11-29" @default.
- W2901636194 creator A5010251963 @default.
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- W2901636194 creator A5057904380 @default.
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- W2901636194 date "2019-02-01" @default.
- W2901636194 modified "2023-10-09" @default.
- W2901636194 title "Sedimentology and sequence stratigraphy of the late-Messinian - Early pliocene continental to marine deposits of the Boudinar basin (North Morocco)" @default.
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- W2901636194 doi "https://doi.org/10.1016/j.jafrearsci.2018.11.002" @default.
- W2901636194 hasPublicationYear "2019" @default.
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